锑矿床

  • 网络antimony deposit
锑矿床锑矿床
  1. 贵州半坡锑矿床卤素元素地球化学研究

    On halogen element geochemistry of the Banpo antimony deposit

  2. 湘中锡矿山锑矿床的Sr同位素地球化学

    Strontium isotope geochemistry of the Xikuangshan antimony deposit , Central Hunan

  3. 广东嵩溪银&锑矿床属中低温浅成热液矿床。

    Songxi Ag - Sb deposit belongs to an epithermal deposit .

  4. 钖矿山锑矿床氧化带的基本特征

    The fundamental characteristics of oxidized zone of antimony ore deposit in Xikuangshan

  5. 广东嵩溪银&锑矿床的地质地球化学特征

    Geological and geochemical characteristics of Songxi Ag-Sb deposit in Guangdong

  6. 锡矿山式锑矿床的成矿流体研究

    The Ore - Forming Fluids of Xikuangshan-Type Antimony Deposits

  7. 湘中锡矿山超大型锑矿床的碳、氧同位素体系

    Carbon and Oxygen Isotope Systematics in the Xikuangshan Giant Antimony Deposit , Central Hunan

  8. 中国主要类型锑矿床硫同位素组成及地球化学特征

    The sulfur isotope compositions and geochemical characterisitics of the antimony deposits of main types in China

  9. 认为锑矿床中辉锑矿最佳形成温度为180℃~220℃,盐度变化范围为(5~10)wt%NaCl。

    It is regarded that the most probable temperature of formation for stibnite is from 180 ℃ to 220 ℃, and the salinity ranges from ( 5 ~ 10 ) wt % NaCl .